VIII ENCUENTRO NACIONAL DE ESTUDIANTES DE GEOLOGÍA 6-10 Noviembre 2017 Copiapó, Chile

Total Page:16

File Type:pdf, Size:1020Kb

VIII ENCUENTRO NACIONAL DE ESTUDIANTES DE GEOLOGÍA 6-10 Noviembre 2017 Copiapó, Chile VIII ENCUENTRO NACIONAL DE ESTUDIANTES DE GEOLOGÍA 6-10 Noviembre 2017 Copiapó, Chile CONTRIBUCIONES CIENTÍFICAS Comité organizador del evento BADITH MUÑOZ FRANCO, Presidente ADOLFO MUÑOZ VALDEBENITO, Secretario general EDGARDO HINOJOSA MEZA, Tesorero FELIPE FUENZALIDA ROJO, Alojamiento JORGE ROMERO MOYANO, Comité científico FELIPE VÉLIZ RIVAS, Terrenos SEBASTIÁN GARCÍA ARROYO, Página web GRISEL RIVERA, Comunicaciones MARCELO GIL VICENCIO, Entretenimiento MAXIMILIANO FORCH, Deportes JAVIERA FERNÁNDEZ, Logística charlas FRANCISCA GALILEA LASTRA, Inscripciones JEAN KARLA ZAMBRANA, Suvenir JONATHAN PEREZ, Alimentación Comité editorial DR. MANUEL ABAD, Geomorfología y Sedimentología, Universidad de Atacama DRA. TATIANA IZQUIERDO, Geología Ambiental e Hidrogeología, Universidad de Atacama DR. KARL RIVEROS, Metalogénesis, Universidad de Atacama DR. JUAN DÍAZ-ALVARADO, Geoquímica y Petrogénesis, Universidad de Atacama DR. ENRIQUE BERNARDEZ, Paleontología y Estratigrafía, Universidad de Atacama DR. WOLFGANG GRIEM, Tectónica y Mineralogía, Universidad de Atacama DR. M. AYAZ ALAM, Volcanología, Geotermia e Hidrogeología, Universidad de Atacama DR. GONZÁLO GALAZ, Petrografía Metamórfica y Tectónica, Universidad de Atacama Editores invitados DR. LUIS LARA, Volcanología, Sernageomin MSC. JORGE BUSTILLOS, Volcanología, Universidad Central de Ecuador MSC. LILIANA TRONCOSO, Peligros Geológicos, Universidad Central de Ecuador 2 Patrocina Auspicia Universidades invitadas 3 PROLOGO El Encuentro Nacional de Estudiantes de Geología (ENEGeol) es una iniciativa social, creada y conducida por estudiantes de pregrado, bajo el alero de la Coordinadora Nacional de Estudiantes de Geología (CONACEG) y con el apoyo de las diversas casas de educación superior que imparten la carrera en el país. Se posiciona como una instancia de reunión para todo el alumnado de las carreras de Geología en Chile, que incentiva la interacción entre pares, el intercambio conocimientos científicos, la construcción de plataformas de trabajo, la discusión del rol de las Geociencias en la sociedad del futuro y también la discusión de problemáticas específicas y transversales que afectan a los estudiantes en el país. La VIII entrega de esta noble reunión tiene como sede oficial la Región de Atacama, siendo conducida por los estudiantes de la Carrera de Geología Universidad de Atacama, casa de estudios que además celebra su décimo aniversario de fundación de la carrera. Instalado en el margen más austral del desierto más árido del mundo, la geología, los contrastes y bellezas cautivantes de Atacama reciben a los más de 400 participantes con fraternidad, alegría y orgullo. Esta instancia además, resalta cuán fundamental es la interacción Geociencias- sociedad, en el contexto de una Región fuertemente azotada por los más grandes aluviones de los últimos 20 años en el Norte de Chile (Marzo 2015 y Mayo 2017). La presente versión ENEGeol 2017 es el resultado del trabajo incesante y desinteresado de un gran número de alumnos, profesores, autoridades e instituciones. Con ello, en este Libro de Contribuciones se presentan 30 investigaciones inéditas, que se suman a las 32 conferencias ofrecidas por alumnos e investigadores, 4 cursos especializados y 9 visitas a terreno al interior de la Región. Esperamos que los recuerdos de este encuentro perduren a través del tiempo geológico. Comité organizador del evento 4 CONTENIDOS Presentaciones invitadas Andrés Folguera , Guido Gianni, Cesar Navarrete, Andrés Echaurren, Lucas Fennell, Darío Orts, Lucía Fernández Paz, Sofía Iannelli, Vanesa Litvak y Alfonso Encinas Construcción de los Andes Patagónicos desde el Jurásico medio hasta el presente........................ 8 Brent Alloway The recognition, correlation and characterization of tephra subjected to intense post-depositional weathering & disturbance in temperate- to tropical-climate environments: A case study from the wet, hyper-humid environment of northwestern Patagonia............................................................. 12 Brent Alloway No small feet: Tracing the footsteps of Southeast Asia's earliest hominins using tephrochronology. 13 Reynaldo Charrier La carrera de Geología. Situación actual y temas pendientes......................................................... 14 Eduardo Campos Aplicaciones de inclusiones fluidas en metalogénesis..................................................................... 20 Tatiana Izquierdo ¿Es el cambio climático el culpable de los últimos aluviones en Copiapó? Primeras respuestas del proyecto COPIFLOOD...................................................................................................................... 22 Felipe Orellana Las rocas máficas y ultramáficas de la serie occidental en el centro sur de chile (39-40°S)............ 23 Felipe Orellana Los desastres no son naturales....................................................................................................... 24 Jorge Bustillos Fifteen years of ash memoirs at Tungurahua volcano, Ecuador....................................................... 25 5 Sesiones regulares (poster y charla) Franco Vera y José Luis Palma Avalanchas mixtas y depósitos proximales generados en la erupción de 2015 del Volcán Villarrica y su interacción con la cubierta glacial........................................................................................... 28 Franco Vera y José Luis Palma Origen, transporte y emplazamiento de lahares generados en la erupción de 2015 del Volcán Villarrica......................................................................................................................................... 33 Enrique Crisóstomo y Fabián Figueroa Estudio petrográfico y de proveniencia de rocas arqueológicas de la zona de Antofagasta (S23°42’-24°12’), Chile.................................................................................................................. 38 Jorge E. Romero, Frederick Swanson, Brent Alloway, Mauricio Mella, Sebastian Watt, David Pyle, Daniele Morgavi , Fabio Arzilli, Romina Daga, Jorge Bustillos, Alicia Guevara, Juan Díaz-Alvarado y Evelyn Cuenca Observaciones preliminares de la tefroestratigrafía en el flanco norte del volcán Calbuco, Andes del Sur (Chile)................................................................................................................................. 44 Rayen Gho, Pablo Forte, Jorge Romero, Constanza Perales, Mariana P. Jácome, Gino González, Emilce Bustos, Francisco Vásconez, Ivonne Lazarte y Diana Rodríguez La volcanología chilena en el contexto latinoamericano: estado actual y perspectivas para las nuevas generaciones...................................................................................................................... 49 Felipe Reinoso y Juan Díaz-Alvarado Resultados preliminares del análisis estructural y petrográfico de "El Caos de Puquios"................. 54 Francisca Ampuero, Jhonny Bahamondes, Ignacio Bernard, Erick Cifuentes, Enrique Crisóstomo, Yael Hernández, Constanza Jorquera, Catalina Larrère, Pablo Morales, Verónica Oliveros, Constanza Perales, Claudio Schulz, José Sepúlveda, René Thibaut, Matías Valencia y Esteban Yévenes Caracterización isotópica mediante δ8O y δ2H de la cuenca del río Biobío, VIII región, Chile................................................................................................................................... 59 Leslie Guajardo y Verónica Oliveros Pseudotaquilitas en brechas de mélange dentro de un prisma de acreción.................................... 64 Nicolás Luengo, Jorge Romero, Daniel Basualto, Luis E. Lara y José Luis Palma Resultados preliminares de la actividad explosiva 2016-2017 del Complejo Volcánico Nevados de Chillán, región del Ñuble................................................................................................................. 70 Suan-lin Lock Geomorfología de tsunami: formas y depósitos generados por el Tsunami del 16 de Septiembre de 2015 en la Bahía de Coquimbo, IV Región de Coquimbo, Chile................................................. 76 Javiera Cifuentes Evaluación de la vulnerabilidad ante el impacto de tsunami de los núcleos urbanos costeros de la Región de Atacama (Chile)............................................................................................................ 81 Nicole Maldonado Patrimonio Geológico del Sector Costero de Caldera, Atacama Chile............................................. 86 Sebastián Cabrera, Camila Jiménez, Andrés Tassara Análisis de efectos climáticos y reológicos en la deformación cortical en Chile.............................. 91 6 Sebastián Galleguillos Análisis y cartografía de procesos geológicos peligrosos en Chañaral (Atacama, Chile).................. 95 Carolina Zapata Proyecto VTT Magma Nüyün.......................................................................................................... 99 Karyme Soleman, Edgardo Hinojosa, Ariel Godoy, Gerardo Castillo, Camila Palacio, Enrique Bernárdez y Manuel Abad Estudio geológico y paleontológico preliminar del yacimiento Los Dedos (Neógeno, Atacama)........ 100 Nicoll Castillo y Miguel Tapia Proyecto FIC “Geoturismo en el Valle del Huasco. Un aporte de las geociencias al desarrollo y crecimiento del turismo tradicional”............................................................................................... 106 Nadia Jara, Javiera Jiménez, Andrés Tassara, Francisco García Campo de deformación superficial del margen Andino (18-45°S) desde vectores de velocidad GNSS.............................................................................................................................................
Recommended publications
  • The Socioeconomic Consequences of Natural Disasters in Chile
    The Socioeconomic Consequences of Natural Disasters in Chile Item Type text; Electronic Thesis Authors Christensen, Rachel Julia Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 06/10/2021 09:06:12 Item License http://rightsstatements.org/vocab/InC/1.0/ Link to Item http://hdl.handle.net/10150/624942 THE SOCIOECONOMIC CONSEQUENCES OF NATURAL DISASTERS IN CHILE By RACHEL JULIA CHRISTENSEN ____________________ A Thesis Submitted to The Honors College In Partial Fulfillment of the Bachelors degree With Honors in Economics THE UNIVERSITY OF ARIZONA MAY 2 0 1 7 Approved by: ____________________________ Dr. Todd Neumann Department of Economics Christensen 2 ABSTRACT: The aim of this project is to analyze the economic effects over time that Chile has encountered due to natural disasters. I will provide information about Chile as country, breaking down several crucial regions to highlight the key threats to each. Several natural disasters used in my research will be defined and a brief account of their occurrences throughout the country’s history will be given. My paper will demonstrate how Chilean society has shaped their way of life around these economic consequences, with a unique look at the short-term effects on small businesses. The primary focus will be on how the economic impact of an exogenous variable, such as a natural disaster, varies based on certain endogenous variables such as location and prosperity.
    [Show full text]
  • Sr–Pb Isotopes Signature of Lascar Volcano (Chile): Insight Into Contamination of Arc Magmas Ascending Through a Thick Continental Crust N
    Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera To cite this version: N. Sainlot, I. Vlastélic, F. Nauret, S. Moune, F. Aguilera. Sr–Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust. Journal of South American Earth Sciences, Elsevier, 2020, 101, pp.102599. 10.1016/j.jsames.2020.102599. hal-03004128 HAL Id: hal-03004128 https://hal.uca.fr/hal-03004128 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright Manuscript File Sr-Pb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust 1N. Sainlot, 1I. Vlastélic, 1F. Nauret, 1,2 S. Moune, 3,4,5 F. Aguilera 1 Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, F-63000 Clermont-Ferrand, France 2 Observatoire volcanologique et sismologique de la Guadeloupe, Institut de Physique du Globe, Sorbonne Paris-Cité, CNRS UMR 7154, Université Paris Diderot, Paris, France 3 Núcleo de Investigación en Riesgo Volcánico - Ckelar Volcanes, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 4 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avenida Angamos 0610, Antofagasta, Chile 5 Centro de Investigación para la Gestión Integrada del Riesgo de Desastres (CIGIDEN), Av.
    [Show full text]
  • Pore-Water in Marine Sediments Associated to Gas Hydrate Dissociation Offshore Lebu, Chile. Carolina Cárcamo1,2, Iván Vargas-C
    Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-362 Manuscript under review for journal Hydrol. Earth Syst. Sci. Discussion started: 29 August 2018 c Author(s) 2018. CC BY 4.0 License. 1 Pore-water in marine sediments associated to gas hydrate dissociation 2 offshore Lebu, Chile. 3 4 Carolina Cárcamo1,2, Iván Vargas-Cordero1, Francisco Fernandoy1, Umberta 5 Tinivella3, Diego López-Acevedo4, Joaquim P. Bento5, Lucía Villar-Muñoz6, Nicole 6 Foucher1, Marion San Juan1, Alessandra Rivero1 7 8 1 Universidad Andres Bello, Facultad de Ingeniería, Quillota 980, Viña del Mar, Chile 9 2 Centro de Investigación Marina Quintay. CIMARQ. Facultad de Ciencias de la Vida. Universidad 10 Andres Bello, Viña del Mar, Chile. 11 3 OGS Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Borgo Grotta Gigante 42/C, 12 34010, Sgonico, Italy. 13 4 Universidad de Concepción, Departamento de Oceanografía, Programa COPAS Sur-Austral, 14 Campus Concepción Víctor Lamas 1290, P.O. Box 160-C, Concepción, Chile 15 5 Escuela de Ciencias del Mar, Pontificia Universidad Católica de Valparaíso, Av. Altamirano 1480, 16 2360007 Valparaíso, Chile. 17 6 GEOMAR Helmholtz Centre for Ocean Research, Wischhofstr. 1-3, 24148 Kiel, Germany. 18 19 ABSTRACT 20 Gas hydrate occurrences along the Chilean margin has been documented, but the 21 processes associated to fluid escapes originated by gas hydrate dissociation yet are 22 unknown. Here, we report morphologies growing related to fluid migration in the 23 continental shelf offshore western Lebu (37 °S) by analysing mainly geochemical 24 features. In this study oxygen and deuterium stable water isotopes in pore water 25 were measured.
    [Show full text]
  • Holocene Event Record of Aysén Fjord (Chilean Patagonia): An
    Holocene Event Record of Aysén Fjord (Chilean Patagonia): An Interplay of Volcanic Eruptions and Crustal and Megathrust Earthquakes Katleen Wils, Maarten van Daele, Galderic Lastras, Catherine Kissel, Frank Lamy, Giuseppe Siani To cite this version: Katleen Wils, Maarten van Daele, Galderic Lastras, Catherine Kissel, Frank Lamy, et al.. Holocene Event Record of Aysén Fjord (Chilean Patagonia): An Interplay of Volcanic Eruptions and Crustal and Megathrust Earthquakes. Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2018, 123 (1), pp.324 - 343. 10.1002/2017JB014573. hal-01791462 HAL Id: hal-01791462 https://hal.archives-ouvertes.fr/hal-01791462 Submitted on 17 Sep 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Holocene Event Record of Aysén Fjord (Chilean Patagonia): 10.1002/2017JB014573 An Interplay of Volcanic Eruptions and Crustal Key Points: and Megathrust Earthquakes • Paleoseismic strategy based on fjord sediments Katleen Wils1 , Maarten
    [Show full text]
  • Redalyc.Seismic-Stratigraphic Architecture of the Oligocene
    Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Alván, Aldo; Criales, Astrid; von Eynatten, Hilmar; Dunkl, Istvan; Gerdes, Axel; Jacay, Javier Seismic-stratigraphic architecture of the Oligocene-Pliocene Camaná Formation, southern Peruvian forearc (Province of Arequipa) Andean Geology, vol. 44, núm. 1, enero, 2017, pp. 17-38 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173949489002 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 44 (1): 17-38. January, 2017 Andean Geology doi: 10.5027/andgeoV44n1-a02 www.andeangeology.cl Seismic-stratigraphic architecture of the Oligocene-Pliocene Camaná Formation, southern Peruvian forearc (Province of Arequipa) Aldo Alván1,2,5, Astrid Criales3, Hilmar von Eynatten2, Istvan Dunkl2, Axel Gerdes4, Javier Jacay5 1 Laboratorio BIZALAB, Calle Aldabas No 626, Santiago de Surco, Lima, Perú. [email protected] 2 University of Göttingen, Geoscience Center, Department of Sedimentology and Environmental Geology, Goldschmidtstrasse 3, D-37077, Germany. [email protected]; [email protected] 3 Universidad de San Martín de Porres, Laboratorio de Investigación Aplicada, Facultad de Ingeniería y Arquitectura. Avda. La Fontana 1250, La Molina, Lima, Perú. [email protected] 4 University of Frankfurt, Institute of Geosciences, Altenhofer Allee 1, D-60431, Germany. [email protected] 5 Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica.
    [Show full text]
  • Gas Hydrate Versus Seabed Morphology Offshore Lebu
    www.nature.com/scientificreports OPEN Gas hydrate versus seabed morphology ofshore Lebu (Chilean margin) Iván Vargas‑Cordero1*, Umberta Tinivella2, Lucía Villar‑Muñoz3,4, Joaquim P. Bento5, Carolina Cárcamo6, Diego López‑Acevedo5, Francisco Fernandoy6, Alessandra Rivero6 & Marion San Juan6,7 Gas‑hydrate occurrences along the Chilean margin have been widely documented, but the processes associated with fuid escapes caused by the dissociation of gas hydrates are still unknown. We report a seabed morphology growth related to fuid migration ofshore Lebu associated with mud cones by analysing oxygen and deuterium stable water isotopes in pore water, bathymetric, biological and sedimentological data. A relief was observed at − 127 m water depth with fve peaks. Enrichment values of δ18O (0.0–1.8‰) and δD (0.0–5.6‰) evidenced past hydrate melting. The orientation of the relief could be associated with faults and fractures, which constitute pathways for fuid migration. The benthic foraminifera observed can be associated with cold seep areas. We model that the mud cones correspond to mud growing processes related to past gas‑hydrate dissociation. The integration of (i) the seismic data analysis performed in the surrounding area, (ii) the orientation of our studied relief, (iii) the infaunal foraminifera observed, (iv) the grain size and (v) the total organic matter and isotope values revealed that this area was formerly characterised by the presence of gas hydrates. Hence, this part of the Chilean margin represents a suitable area for investigating fuid‑migration processes. Along continental margins, morphological features associated with fuid escapes such as mud volcanoes, mud mounds, pockmarks, seeps, precipitates—carbonates and hydrates-, piping/rills and brine pools have been reported worldwide (e.g.1–7).
    [Show full text]
  • U-Pb Geochronology and Paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-Scale
    Research Paper GEOSPHERE U-Pb geochronology and paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-scale GEOSPHERE, v. 17, no. 1 source areas https://doi.org/10.1130/GES02284.1 E. Schwarz1,*, E.S. Finzel2,*, G.D. Veiga1, C.W. Rapela1, C. Echevarria3,*, and L.A. Spalletti1 1Centro de Investigaciones Geológicas (Universidad Nacional de La Plata–Consejo Nacional de Investigaciones Científicas y Técnicas [CONICET]), Diagonal 113 #256 B1904DPK, La Plata, Argentina 13 figures; 2 tables; 1 set of supplemental files 2Earth and Environmental Science Department, University of Iowa, 115 Trowbridge Hall, Iowa City, Iowa 52242, USA 3Pampa Energía S.A. Gerencia Tight, Dirección de E&P, J.J. Lastra 6000, 8300 Neuquén, Argentina CORRESPONDENCE: [email protected] ABSTRACT starting in the mid-continent region of south- Early Cretaceous was the Neuquén Basin, which CITATION: Schwarz, E., Finzel, E.S., Veiga, G.D., western Gondwana and by effective sorting, was during that time was a backarc basin separated Rapela, C.W., Echevarria, C., and Spalletti, L.A., Sedimentary basins located at the margins bringing fine-grained or finer caliber sand to the from the proto–Pacific Ocean (i.e., to the west) by 2021, U-Pb geochronology and paleogeography of the of continents act as the final base level for con- Neuquén Basin shoreline. This delivery system was a discontinuous volcanic arc (Howell et al., 2005). Valanginian–Hauterivian Neuquén Basin: Implications for Gondwana-scale source areas: Geosphere, v. 17, tinental-scale catchments that are sometimes probably active (though not necessarily continu- This marine basin was bounded by the Sierra no.
    [Show full text]
  • Tectonic Implications of Late Cenozoic Sedimentation from the Coastal Cordillera of Northern Chile (22-24"S)
    Journal ofrhe Geological Sociery, London, Vol. 152, 1995, pp. 51-63, 11 figs, 1 table. Printed in Northern Ireland Tectonic implications of Late Cenozoic sedimentation from the Coastal Cordillera of northern Chile (22-24"s) A. J. HARTLEY' & E. J. JOLLEY2 'Production Geoscience Research Unit, Department of Geology and Petroleum Geology, University of Aberdeen, Aberdeen AB9 2UE, UK 'BP Exploration, Farburn Industrial Estate, Dyce, Aberdeen AB2 OPB, UK Abstract: Late Cenozoic sediments from northern Chile (22-24"s) are exposed on the coastal plain between the Coastal Cordillera to the east and tilted fault blocks of the Mejillones Peninsula to the west. During the mid-Miocene to Pliocene (?up to mid-Pleistocene) a shallow marine basin developed unconformably over basement. Sedimentation was initially restricted to a small half-graben on the western margin of the Mejillones Peninsula during the Miocene. Expansion of the basin during the early Pliocene resulted in widespread shallow marine sedimentation across the study area. Alluvial, aeolian and beach sediments were restricted to the basin margins, where sediment was supplied from the Coastal Scarp (a major cliff-line bounding the western margin of the Coastal Cordillera) and isolated(islands) fault blocks. Areas of restrictedclastic input were characterized by carbonate deposition. Marine planation surfaces or terraces (0.5-600m elevation) and associated palaeo-sea cliffs cut intoMiocene-Pliocene sediments and basement rocks, developed along the coastline of northern Chile in the ?late Pliocene to late Pleistocene. A similar age for a number of late Pleistocene terraces (125 OOO years) now at different elevations, suggests that they were cut during interglacial highstands (oxygen isotope stage 5).
    [Show full text]
  • Overview of Chaitén Volcano, Chile, and Its 2008-2009 Eruption
    Andean Geology 40 (2): 196-215. May, 2013 Andean Geology doi: 10.5027/andgeoV40n2-a01 formerly Revista Geológica de Chile www.andeangeology.cl Overview of Chaitén Volcano, Chile, and its 2008-2009 eruption Jon J. Major1, Luis E. Lara2 1 United States Geological Survey, Cascades Volcano Observatory, 1300 SE Cardinal Court, Vancouver, Washington, 98683, USA. [email protected] 2 Servicio Nacional de Geología y Minería, Programa de Riesgo Volcánico, Avda. Santa María 0104, Santiago, Chile. [email protected] ABSTRACT. Chaitén Volcano erupted unexpectedly in May 2008 in one of the largest eruptions globally since the 1990s. It was the largest rhyolite eruption since the great eruption of Katmai Volcano in 1912, and the first rhyolite eruption to have at least some of its aspects monitored. The eruption consisted of an approximately 2-week-long explosive phase that generated as much as 1 km3 bulk volume tephra (~0.3 km3 dense rock equivalent) followed by an approximately 20-month-long effusive phase that erupted about 0.8 km3 of high-silica rhyolite lava that formed a new dome within the volcano’s caldera. Prior to its eruption, little was known about the eruptive history of the volcano or the hazards it posed to society. This edition of Andean Geology contains a selection of papers that discuss new insights on the erup- tive history of Chaitén Volcano, and the broad impacts of and new insights obtained from analyses of the 2008-2009 eruption. Here, we summarize the geographic, tectonic, and climatic setting of Chaitén Volcano and the pre-2008 state of knowledge of its eruptive history to provide context for the papers in this edition, and we provide a revised chronol- ogy of the 2008-2009 eruption.
    [Show full text]
  • Tectonic Control of the Geothermal System at Mt. Villarrica - Insights from Geophysical and Geochemical Surveys
    O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Tectonic control of the geothermal system at Mt. Villarrica - Insights from geophysical and geochemical surveys Sebastian Held1*, Eva Schill2, Maximiliano Pavez3,5, Daniel Diaz3,5, Diego Morata4,5 and Thomas Kohl1 1Institute of Applied Geosciences, Karlsruhe Institute of Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, Germany 2Institute for Nuclear Waste Disposal, Karlsruhe Institute of Technology (KIT), Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, Germany 3Departament of Geophysics, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Chile 4Departament of Geology, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Chile 5Centro de Excellencia en Geotermina de Los Andes (CEGA), Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile *Contact email: [email protected] Abstract. Geothermal systems are often related to active products are absent (Held et al., 2015). volcanic areas forming typical high-enthalpy geothermal The tectonic situation, including the over 1200 km long N- reservoirs. However at Mt. Villarrica the processes active in S aligned LOFS, may be responsible for the absence of a the subsurface do not favor the formation of high-enthalpy high-enthalpy geothermal reservoir in the vicinity of one of geothermal reservoirs. Geophysical and geochemical the most active volcanoes of Chile (Ortiz, 2003). However, investigations demonstrate the importance of major faults the origin and possible flow paths of the geothermal fluid governing fluid flow in the subsurface.
    [Show full text]
  • Control Estructural Del Basamento Sobre El Volcanismo Cuaternario Del Complejo Volcánico Chaitén- Michinmahuida
    1 Control estructural del basamento sobre el volcanismo Cuaternario del Complejo Volcánico Chaitén- Michinmahuida Memoria para optar al Título de Geólogo Ramiro Alejandro Muñoz Ramírez Concepción, 2019 2 Control estructural del basamento sobre el volcanismo Cuaternario del Complejo Volcánico Chaitén- Michinmahuida Memoria para optar al Título de Geólogo Ramiro Alejandro Muñoz Ramírez Profesor Patrocinante: Dr. Andrés Humberto Tassara Oddo Profesores Comisión: Dr. Jorge Andrés Quezada Flory MSc. Abraham Elías González Martínez Concepción, 2019 3 A mis padres y familia 4 ÍNDICE Página RESUMEN……………………………………………………………………………….. 1. INTRODUCCIÓN ………………………………………………………….…... 1 1.1. Generalidades …………………………………………………………... 1 1.2. Objetivos …………………………………………………………………. 3 1.2.1. Objetivo general …………………………………………………. 3 1.2.2. Objetivos específicos …………………………………………...... 3 1.3. Ubicación y accesos ……………………………………………………. 3 1.4. Trabajos anteriores …………………………………………………… 4 1.5. Agradecimientos ……………………………………………………….. 9 2. MARCO TEÓRICO Y METODOLOGÍA ……………………………….. 10 2.1. Conceptos teóricos …………………………………………………….. 10 2.1.1. Conceptos para análisis cinemático …………………………….. 10 2.1.2. Conceptos para análisis dinámico ……………………………… 13 2.2. Metodología de trabajo ……………………………………………..... 15 2.2.1. Compilación y análisis de sistemas de información …………… 15 2.2.2. Obtención de datos en terreno ………………………………….. 15 2.2.3. Procesamiento de datos de terreno …………..…………………. 18 3. MARCO GEOLÓGICO ………………………………………………………. 22 3.1. Marco geológico regional ………………………………………......... 22 3.1.1. Rocas Metamórficas (Pz-Tr)-CMAP …………………………… 24 3.1.2. Intrusivo Devónico (Dg)-Metatonalita Chaitén ……………...... 26 3.1.3. Intrusivo Pérmico-Triásico(PTrg) .……………………………... 27 3.1.4. Intrusivo Cretácico (Kg)-Batolito Norpatagónico Kg ………… 27 3.1.5. Intrusivo Mioceno (Mg)-Batolito Norpatagónico Mg …………. 28 3.1.6. Fomarción volcano-sedimentaria Ayacara-Puduguapi (EsOva) 29 3.1.7. Estratos de Llahuén (Plill) …………………………….………… 30 3.2.8.
    [Show full text]
  • Cretaceous-Cenozoic Growth of the Patagonian Broken Foreland Basin
    Journal of South American Earth Sciences 97 (2020) 102242 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Cretaceous-Cenozoic growth of the Patagonian broken foreland basin, T Argentina: Chronostratigraphic framework and provenance variations during transitions in Andean subduction dynamics ∗ Kristina L. Butlera,b, , Brian K. Hortona,b, Andrés Echaurrenc, Andrés Folguerac, Facundo Fuentesd a Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA b Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA c Instituto de Estudios Andinos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires-CONICET, Buenos Aires, Argentina d YPF S.A., 515 Macacha Güemes, Buenos Aires, Argentina ARTICLE INFO ABSTRACT Keywords: The Cretaceous-Cenozoic evolution of the Patagonian broken foreland basin system at 42–43°S in the northern Andes Chubut province of Argentina is associated with variable retroarc phases of fold-thrust belt shortening, exten- Patagonia sion, and basement uplift during changes in the dynamics of oceanic slab subduction. Basement inheritance and Foreland basin progressive shallowing of an east-dipping subducting slab are important mechanisms of foreland partitioning, as Provenance dictated by the preexisting (pre-Andean) structural architecture and forelandward (eastward) advance of Late U-Pb geochronology Cretaceous arc magmatism. Previously recognized growth strata help define the timing of fold-thrust belt Hf isotopes shortening and retroarc basement-involved uplift, but the precise consequences for sediment routing remain poorly understood, with uncertainties in patterns of basin evolution before, during, and after shallowing and resteepening of the subducting slab.
    [Show full text]